Marichuela Formation

Marichuela Formation Stratigraphic range: Late Miocene-Early Pliocene ~8.2–5 Ma PreЄ Є O S D C P T J K Pg N ↓
Type	Geological formation
Underlies	Tilatá Formation
Overlies	Guadalupe Group
Thickness	up to 40 metres (130 ft)
Lithology
Primary	Conglomerate
Location
Coordinates	4°21′40.3″N 74°07′50″W / 4.361194°N 74.13056°W / 4.361194; -74.13056Coordinates: 4°21′40.3″N 74°07′50″W / 4.361194°N 74.13056°W / 4.361194; -74.13056
Region	Bogotá savanna, Altiplano Cundiboyacense Eastern Ranges, Andes
Country	Colombia
Type section
Named for	Marichuela neighbourhood
Named by	Helmens & Hammen
Location	Usme, Bogotá
Year defined	1995
Coordinates	4°21′40.3″N 74°07′50″W / 4.361194°N 74.13056°W / 4.361194; -74.13056
Region	Cundinamarca
Country	Colombia

The Marichuela Formation (Spanish: Formación Marichuela, N_1m) is a geological formation of the Bogotá savanna, Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The formation consists of coarse to very coarse conglomerates. The Marichuela Formation dates to the Neogene period; Late Miocene to Early Pliocene epochs, and has a maximum thickness of 40 metres (130 ft).

Etymology

The formation was defined by Helmens and Van der Hammen in 1995 and named after the Marichuela neighbourhood of Usme.^[1] Part of the Marichuela Formation had been included in the Conos de Tunjuelo, defined by Julivert in 1961.^[2]

Description

Lithologies

The Marichuela Formation consists of coarse to very coarse conglomerates.^[1]

Stratigraphy and depositional environment

The Marichuela Formation unconformably overlies the Cretaceous rocks of the Guadalupe Group. The age has been estimated to be Late Miocene to Early Pliocene.^[3] The depositional environment has been interpreted as alluvial fans, caused by earthquakes or heavy rains.^[4]

Outcrops

Type locality of the Marichuela Formation to the southeast of the Bogotá savanna

The Marichuela Formation is apart from its type locality in the Usme Synclinal, the valley of the Tunjuelo River, found in the synclinals of Neusa, Sisga and La Calera.^[1]

See also

Geology of the Eastern Hills

Geology of the Ocetá Páramo

Geology of the Altiplano Cundiboyacense

References

Bibliography

• Montoya Arenas, Diana María, and Germán Alfonso Reyes Torres. 2005. Geología de la Sabana de Bogotá, 1–104. INGEOMINAS.
• N., N. s.a. Parque Ecológico Distrital de Montaña Entrenubes – Tomo I – Componente Biofísico – Geología, 36–51. Corporación Suna Hisca.

Maps

• Buitrago, José Alberto; Roberto Terraza M., and Fernando Etayo. 1998. Plancha 228 - Santafé de Bogotá Noreste - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.

External links

• Gómez, J.; N.E. Montes; Á. Nivia, and H. Diederix. 2015. Plancha 5-09 del Atlas Geológico de Colombia 2015 – escala 1:500,000, 1. Servicio Geológico Colombiano. Accessed 2017-03-16.